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Geology; October 2005; v. 33; no. 10; p. 769-772; DOI: 10.1130/G21671.1
© 2005 Geological Society of America
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Grenville-age magmatism at the South Tasman Rise (Australia): A new piercing point for the reconstruction of Rodinia

A.M. Fioretti1, L.P. Black2, J. Foden3 and D. Visonà4

1 Consiglio Nazionale delle Ricerche (CNR), Istituto di Geoscienze e Georisorse, Corso Garibaldi 37, I-35137 Padova, Italy, and Visiting Fellows at Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia
2 Minerals Division, Geoscience Australia, GPO Box 378, Canberra, ACT 2601, Australia, and Visiting Fellows at Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia
3 Department of Geology and Geophysics, University of Adelaide, Adelaide, SA 5005, Australia
4 Dipartimento di Mineralogia e Petrologia, Università di Padova, Corso Garibaldi 37, I-35137 Padova, Italy

A U-Pb zircon sensitive high-resolution ion microprobe age of 1119.4 ± 8.5 Ma, obtained from a quartz syenite dredged from the South Tasman Rise (Australia), provides the first direct evidence of the presence of Grenville-age magmatic rocks along the central part of the hypothesized Australia–East Antarctica conjugate margin of Laurentia. The distinctive mineralogy and geochemistry of the rock and its Sm-Nd and Pb isotopic signatures 1) indicate that it represents a juvenile Grenville-age addition to the crust, 2) support a correlation with the Grenville magmatic province of the western United States, and 3) set a unique pivotal point for a precise reconstruction of Rodinia. The resulting scenario implies the presence of a new magmatic province crossing the East Antarctic craton, the extension of Proterozoic belts of southwest Laurentia to East Antarctica, and appears consistent with the Australia–western United States (AUSWUS) model. This tectonic setting envisages a near-local source for the ubiquitous Grenville-age detrital zircon population in marginal Neoproterozoic to early Paleozoic Gondwanan sequences and suggests a possible direct source for the widespread Grenville-age inherited zircon component observed in most Paleozoic granites in northern Victoria Land (Antarctica) and east Tasmania (Australia).

Key Words: South Tasman Rise • Rodinia • Grenville • East Antarctic craton • SHRIMP







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